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Titlebook: Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China; YanJing Chen,Franco Pirajno,YongFei Yang Book 2022 The E

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書目名稱Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China
編輯YanJing Chen,Franco Pirajno,YongFei Yang
視頻videohttp://file.papertrans.cn/384/383370/383370.mp4
概述Covers all molybdenum deposit types, which are contained by Qinling Orogen, the world’s largest molybdenum province.Details fluid flow, metallogenesis and magmatism during continental collision.Propos
叢書名稱Modern Approaches in Solid Earth Sciences
圖書封面Titlebook: Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China;  YanJing Chen,Franco Pirajno,YongFei Yang Book 2022 The E
描述.This book is the first systematic treatise of available data and view-points obtained from geological and geochemical studies of the Mo deposits in Qinling Orogen, China. Qinling Orogen has a minimum reserve of 8.7 Mt Mo, ranking the largest molybdenum province both in China and the world. Incorporating all known Mo deposit types in the world, it presents extensive studies of Mo deposits of world-class and unusual types within tectonic settings. The Qinling Orogen was finally formed during continental collision between Yangtze and North China cratons, following the Triassic closure of the northernmost paleo-Tethys. It hosts 49 Mo deposits formed in seven mineralization events since 1850 Ma, with all the world-class deposits being formed during 160-105 Ma, coeval with collisional orogeny. These deposits are assigned to magmatic and metamorphic hydrothermal classes. The magmatic hydrothermal class includes porphyries, skarns, and intrusion-related veins (carbonatite, fluorite and quartz). The porphyry Mo systems in Qinling Orogen are predominated by Dabie-type formed in continental collision setting, followed by Endako- and Climax-types formed in continental arcs and rifts, respecti
出版日期Book 2022
關(guān)鍵詞Continental Collision and Geochronology; Fluid Inclusions and Molybdenum Deposit; Isotope Geochemistry
版次1
doihttps://doi.org/10.1007/978-981-16-4871-7
isbn_ebook978-981-16-4871-7Series ISSN 1876-1682 Series E-ISSN 1876-1690
issn_series 1876-1682
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Singapor
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Porphyry Mo Deposits,tal collision orogens, respectively. PMDs in Qinling Orogen include Endako- and Dabie-types. The Indosinian PMDs belong to Endako-type, as exemplified by Wenquan deposit. They are limited to the South Qinling Fold Belt, associated with (high-K) calc-alkaline granitic porphyries developed in a contin
地板
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,Porphyry–Skarn Mo Systems,uaxiong Block (HXB), followed by the South Qinling Fold Belt (SQL) and North Qinling Accretion Belt (NQL). The deposits in SQL or NQL are small-sized and contain Cu as by-product, while in HXB, they can be large to giant in size and contain tungsten as by-product. Compared with monotonous porphyry s
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Magmatic-Hydrothermal Vein Systems,resented by the Zhaiwa, Tumen and Huanglongpu deposits, which are introduced in this chapter. They yield pre-Yanshanian ages’ events and provide insights into pre-Yanshanian multistage Mo mineralization and enrichment..The Zhaiwa Mo-Cu-bearing quartz veins were formed by high-salinity magmatic fluid
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Mineralization and Its Controls,sive Mo mineralization occurred in Yanshanian, associated with granitoids. Early Precambrian rocks and their derivative sediments have high Mo concentrations and host giant and large Mo deposits. Physicochemical features of country rocks control mineralization types, locations, and metal inventories
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